سامانه مدیریت نشریات علمی دانشگاه دامغان

صامتی, منا, زمانیان, حسن, اسدی هارونی, هوشنگ. (1399). بررسی زمین شیمیایی و میانبار سیال مس-طلای فراگرمایی کالچویه در بخش میانی کمان ماگمایی ارومیه-دختر. مجله زمین شیمی ایران, 28(1), 217-232. doi: 10.29252/ijcm.28.1.217
منا صامتی; حسن زمانیان; هوشنگ اسدی هارونی. "بررسی زمین شیمیایی و میانبار سیال مس-طلای فراگرمایی کالچویه در بخش میانی کمان ماگمایی ارومیه-دختر". مجله زمین شیمی ایران, 28, 1, 1399, 217-232. doi: 10.29252/ijcm.28.1.217
صامتی, منا, زمانیان, حسن, اسدی هارونی, هوشنگ. (1399). 'بررسی زمین شیمیایی و میانبار سیال مس-طلای فراگرمایی کالچویه در بخش میانی کمان ماگمایی ارومیه-دختر', مجله زمین شیمی ایران, 28(1), pp. 217-232. doi: 10.29252/ijcm.28.1.217
صامتی, منا, زمانیان, حسن, اسدی هارونی, هوشنگ. بررسی زمین شیمیایی و میانبار سیال مس-طلای فراگرمایی کالچویه در بخش میانی کمان ماگمایی ارومیه-دختر. مجله زمین شیمی ایران, 1399; 28(1): 217-232. doi: 10.29252/ijcm.28.1.217

بررسی زمین شیمیایی و میانبار سیال مس-طلای فراگرمایی کالچویه در بخش میانی کمان ماگمایی ارومیه-دختر

مجله بلورشناسی و کانی شناسی ایران
مقاله 15، دوره 28، شماره 1 - شماره پیاپی 77، فروردین 1399، صفحه 217-232    اصل مقاله (4.41 M)
نوع مقاله: مقاله پژوهشی
شناسه دیجیتال (DOI): 10.29252/ijcm.28.1.217
نویسندگان
منا صامتی* 1؛ حسن زمانیان1؛ هوشنگ اسدی هارونی2
1دانشگاه لرستان
2دانشگاه صنعتی اصفهان
چکیده
کانسار مس– طلای کالچویه در بخش مرکزی کمان ماگمایی ارومیه-دختر قرار دارد. میزبان این کانه­زایی بیشتر سنگ­های دیوریتی، کوارتز دیوریتی و آندزیتی هستند. کانه­زایی در مرحله درونزادی با کالکوپیریت، پیریت، گالن و مگنتیت مشخص می­شود که در مرحله برونزاد با ایجاد کالکوسیت، کوولیت، مالاکیت، و گوئتیت ادامه می­یابد. بر اساس بررسی­های زمین شیمیایی، مقدار Lan/Ybn بین 2/2 تا 3/6 و Eu/Eu* از 7/0 تا 1/1 متغیر است. توده­های درونی میزبان کانه­زایی در منطقه کالچویه ویژگی ماگماهای پهنه­­های فرورانش، یعنی غنی­شدگی از عناصر سنگ دوست بزرگ یون (LILE) و تهی شدگی از عناصر با شدت میدان بالا (HFSE) با بی­هنجاری منفی در Ti را نشان می­دهند. داده­های میانبارهای سیال، دمای˚C 310-150، شوری 4-1/0 (درصد وزنی نمک طعام) و ژرفای حدود 400 متر را برای کانه­زایی در کانسار کالچویه نشان می­دهند. روند تکاملی سیال در کانسار کالچویه سردشدگی، رقیق­شدگی سطحی و جوشش را نشان می­دهد. شواهدی از جمله بافت­های نواری و شانه­ای در کوارتز، کلسیت تیغه­ای، برش گرمابی، دگرسانی پروپلیتی و شواهد میانبارهای سیال چون دما و شوری ماهیت فراگرمایی سولفیدشدگی پایین برای کانسار کالچویه را تایید می­کند.     
کلیدواژه‌ها
میانبار سیال؛ سولفیدشدگی پایین؛ فراگرمایی؛ کالچویه؛ ارومیه – دختر
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